Fig Tree Formation
Stromatolite-containing geological formation in South Africa From Wikipedia, the free encyclopedia
The Fig Tree Formation, also called Fig Tree Group, is a stromatolite-containing geological formation in South Africa. The rock contains fossils of microscopic life forms of about 3.26 billion years old.[1] Identified organisms include the bacterium Eobacterium isolatum and the algae-like Archaeosphaeroides barbertonensis. The fossils in the Fig Tree Formation are considered some of the oldest known organisms on Earth, and provide evidence that life may have existed much earlier than previously thought. The formation is composed of shales, turbiditic greywackes, volcaniclastic sandstones, chert, turbiditic siltstone, conglomerate, breccias, mudstones, and iron-rich shales.[2]
Fig Tree Formation | |
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Stratigraphic range: Paleoarchean ~ | |
Type | Geological formation |
Unit of | Barberton Supergroup |
Underlies | Moodies Group |
Overlies | Onverwacht Group |
Lithology | |
Primary | Sandstone |
Other | Shale |
Location | |
Location | Kaapvaal craton |
Coordinates | 25.8°S 31.0°E |
Region | Barberton Greenstone Belt, Mpumalanga |
Country | South Africa |
![]() Location of the Barberton Greenstone Belt |
Meteorite Impact
This formation also contains evidence of the biggest known meteorite impact on earth .
See also
References
Further reading
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